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Defining the Scale to Build Complex Networks with a 40-Year Norwegian Intraplate Seismicity Dataset

We present a new complex network-based study focused on intraplate earthquakes recorded in southern Norway during the period 1980–2020. One of the most recognized limitations of spatial complex network procedures and analyses concerns the definition of adequate cell size, which is the focus of this...

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Autores principales: Pavez-Orrego, Claudia, Pastén, Denisse
Formato: Online Artículo Texto
Lenguaje:English
Publicado: MDPI 2023
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10528423/
https://www.ncbi.nlm.nih.gov/pubmed/37761583
http://dx.doi.org/10.3390/e25091284
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author Pavez-Orrego, Claudia
Pastén, Denisse
author_facet Pavez-Orrego, Claudia
Pastén, Denisse
author_sort Pavez-Orrego, Claudia
collection PubMed
description We present a new complex network-based study focused on intraplate earthquakes recorded in southern Norway during the period 1980–2020. One of the most recognized limitations of spatial complex network procedures and analyses concerns the definition of adequate cell size, which is the focus of this approach. In the present study, we analyze the influence of observational errors of hypocentral and epicentral locations of seismic events in the construction of a complex network, looking for the best cell size to build it and to develop a basis for interpreting the results in terms of the structure of the complex network in this seismic region. We focus the analysis on the degree distribution of the complex networks. We observed a strong result of the cell size for the slope of the degree distribution of the nodes, called the critical exponent [Formula: see text]. Based on the Abe–Suzuki method, the slope ([Formula: see text]) showed a negligible variation between the construction of 3- and 2-dimensional complex networks. The results were also very similar for a complex network built with subsets of seismic events. These results suggest a weak influence of observational errors measured for the coordinates latitude, longitude, and depth in the outcomes obtained with this particular methodology and for this high-quality dataset. These results imply stable behavior of the complex network, which shows a structure of hubs for small values of the cell size and a more homogeneous degree distribution when the cell size increases. In all the analyses, the [Formula: see text] parameter showed smaller values of the error bars for greater values of the cell size. To keep the structure of hubs and small error bars, a better range of the side sizes was determined to be between 8 to 16 km. From now on, these values can be used as the most stable cell sizes to perform any kind of study concerning complex network studies in southern Norway.
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spelling pubmed-105284232023-09-28 Defining the Scale to Build Complex Networks with a 40-Year Norwegian Intraplate Seismicity Dataset Pavez-Orrego, Claudia Pastén, Denisse Entropy (Basel) Article We present a new complex network-based study focused on intraplate earthquakes recorded in southern Norway during the period 1980–2020. One of the most recognized limitations of spatial complex network procedures and analyses concerns the definition of adequate cell size, which is the focus of this approach. In the present study, we analyze the influence of observational errors of hypocentral and epicentral locations of seismic events in the construction of a complex network, looking for the best cell size to build it and to develop a basis for interpreting the results in terms of the structure of the complex network in this seismic region. We focus the analysis on the degree distribution of the complex networks. We observed a strong result of the cell size for the slope of the degree distribution of the nodes, called the critical exponent [Formula: see text]. Based on the Abe–Suzuki method, the slope ([Formula: see text]) showed a negligible variation between the construction of 3- and 2-dimensional complex networks. The results were also very similar for a complex network built with subsets of seismic events. These results suggest a weak influence of observational errors measured for the coordinates latitude, longitude, and depth in the outcomes obtained with this particular methodology and for this high-quality dataset. These results imply stable behavior of the complex network, which shows a structure of hubs for small values of the cell size and a more homogeneous degree distribution when the cell size increases. In all the analyses, the [Formula: see text] parameter showed smaller values of the error bars for greater values of the cell size. To keep the structure of hubs and small error bars, a better range of the side sizes was determined to be between 8 to 16 km. From now on, these values can be used as the most stable cell sizes to perform any kind of study concerning complex network studies in southern Norway. MDPI 2023-08-31 /pmc/articles/PMC10528423/ /pubmed/37761583 http://dx.doi.org/10.3390/e25091284 Text en © 2023 by the authors. https://creativecommons.org/licenses/by/4.0/Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).
spellingShingle Article
Pavez-Orrego, Claudia
Pastén, Denisse
Defining the Scale to Build Complex Networks with a 40-Year Norwegian Intraplate Seismicity Dataset
title Defining the Scale to Build Complex Networks with a 40-Year Norwegian Intraplate Seismicity Dataset
title_full Defining the Scale to Build Complex Networks with a 40-Year Norwegian Intraplate Seismicity Dataset
title_fullStr Defining the Scale to Build Complex Networks with a 40-Year Norwegian Intraplate Seismicity Dataset
title_full_unstemmed Defining the Scale to Build Complex Networks with a 40-Year Norwegian Intraplate Seismicity Dataset
title_short Defining the Scale to Build Complex Networks with a 40-Year Norwegian Intraplate Seismicity Dataset
title_sort defining the scale to build complex networks with a 40-year norwegian intraplate seismicity dataset
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10528423/
https://www.ncbi.nlm.nih.gov/pubmed/37761583
http://dx.doi.org/10.3390/e25091284
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